lithoheterotrophic
METPO:1000648 · CLASS · REVIEWED
A trophic type in which an organism obtains energy from the oxidation of inorganic compounds while using organic compounds as the primary carbon source for biosynthesis.
Lithoheterotrophic inorganic energy and organic carbon use
Edge evidence
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lithoheterotrophic
has electron donor
inorganic electron donor
METPO:2007701Inorganic compounds serve as the energy-generating electron donors for lithoheterotrophy.
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DOI:10.1016/B978-0-12-378630-2.00219-Xoxidize inorganic atoms or molecules
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ferrous iron
example of
inorganic electron donor
rdfs:subClassOfFe(II) is an example inorganic electron donor for lithotrophic growth.
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DOI:10.1038/s41598-021-81412-3Fe(II) as the energy source
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inorganic electron donor
feeds electrons into
respiratory chain
METPO:2007402Oxidation of inorganic donors feeds respiratory electron transport.
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DOI:10.1016/j.bbabio.2008.09.008membrane-bound electron transport chain
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respiratory chain
transfers electrons to
molecular oxygen
METPO:2007403Aerobic Fe(II)-oxidizing lithotrophy can reduce oxygen.
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DOI:10.1038/s41598-021-81412-3oxidation of Fe(II) coupled to the reduction of oxygen
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respiratory chain
has output
ATP
RO:0002234Respiratory electron transport supports ATP synthesis.
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DOI:10.1016/j.bbabio.2008.09.008drives ATP synthesis
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lithoheterotrophic
has carbon source
organic carbon
METPO:2007806Lithoheterotrophy uses organic compounds as carbon sources.
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DOI:10.1038/s41598-021-81412-3glucose as the sole carbon source
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glucose
example of
organic carbon
rdfs:subClassOfGlucose is an experimentally supported organic carbon source.
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DOI:10.1038/s41598-021-81412-3glucose as the sole carbon source
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organic carbon
converted to
precursor metabolites
Organic carbon supplies biosynthetic precursors.
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DOI:10.1038/s41598-021-81412-3biomass precursors provided by glucose
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precursor metabolites
incorporated into
biomass
biolink:part_ofOrganic-carbon precursors are incorporated into cellular material.
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DOI:10.1016/B978-012373944-5.00083-3incorporation of a compound into biomass
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microaerobic conditions
supports
Fe(II) oxidation
Microaerobic conditions support Fe(II)-oxidizing growth by limiting abiotic Fe(II) oxidation.
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DOI:10.1038/s41598-021-81412-3
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ferrous iron
oxidized in
Fe(II) oxidation
Ferrous iron is the substrate oxidized in the energy-yielding Fe(II) oxidation process.
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DOI:10.1038/s41598-021-81412-3
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Fe(II) oxidation
feeds electrons into
respiratory chain
METPO:2007402Fe(II) oxidation provides electrons for respiratory energy conservation.
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DOI:10.1038/s41598-021-81412-3
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sulfide
example of
inorganic electron donor
rdfs:subClassOfSulfide is an inorganic electron donor for lithotrophic sulfur oxidation.
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DOI:10.1038/s41467-025-56588-1
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sulfide:quinone oxidoreductase (SQR)
oxidizes
sulfide
METPO:2007803SQR catalyzes oxidation/detoxification of sulfide as a sulfide-oxidation module.
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DOI:10.1038/s41467-025-56588-1
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thiosulfate
example of
inorganic electron donor
rdfs:subClassOfThiosulfate is an inorganic sulfur electron donor for lithotrophic oxidation.
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DOI:10.1038/s41467-025-56588-1
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periplasmic Sox system
oxidizes
thiosulfate
METPO:2007803The periplasmic Sox system encodes oxidation of thiosulfate.
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DOI:10.1038/s41467-025-56588-1
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conductive pili and c-type cytochromes
enables
direct interspecies electron transfer
RO:0002327Conductive pili and outer-surface c-type cytochromes enable direct interspecies electron transfer.
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DOI:10.3390/life14050591
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Provenance
- Source
- METPO (2025-11-25)
- Author
- Jed Dongjin Kim-Ozaeta
- Definition source
- DOI:10.1038/s41598-021-81412-3
Parent traits (1)
Synonyms (1)
- lithoheterotroph
kg-microbe context
Matched 1 kg-microbe node via direct_metpo.
METPO:1000648[-0.997, -3.520, -5.312, -0.246, …]
Nearest neighbors in embedding space
- physiology trophic type 0.838
- physiology photolithoautotrophic 0.831
- physiology lithoautotrophic 0.829
- physiology hydrogenotrophic 0.827
- physiology carboxydotrophic 0.825
- physiology photoorganoheterotrophic 0.790
- physiology chemoautotrophic 0.783
- physiology mixotrophic 0.777
Deep research
# Curation-focused research report: lithoheterotrophic **Trait:** `lithoheterotrophic` **Identifier:** **“METPO:1000648”** **Category / kind / status:** PHYSIOLOGY / CLASS / REVIEWED **Parent:** `METPO:1000631` ## 1. Scope summary and current understanding Lithoheterotrophy is a trophic strategy in which oxidation of a reduced inorganic electron donor supplies respiratory energy, while preformed organic compounds provide the principal carbon incorporated into biomass. The defining evidence therefore requires two experimentally separable fluxes: **(i)** inorganic-donor oxidation linked to energy conservation and **(ii)** organic-carbon uptake and assimilation. It does not require one universal donor, acceptor, or pathway. The clearest model is *Arcobacter peruensis*: sulfide oxidation is coupled to nitrate reduction, whereas acetate is assimilated and CO₂ fixation is negligible. The isolate grew best with sulfide, nitrate, and acetate; isotope experiments verified acetate assimilation and complete nitrate reduction to N₂. Its reported yield was 3.1 mol assimilated C per mol H₂S oxidized, and sulfide plus acetate supported approximately twice the growth observed under CO₂-fixing conditions. The organism’s acetate system had an apparent *K*m of 5.4 μM. These observations directly separate energy source from biomass-carbon source. (callbeck2019arcobacterperuensissp. pages 9-12) A 2023 marine study broadened this model to trace-gas metabolism: H₂ oxidation by uptake [NiFe]-hydrogenases can supply enough energy for growth of otherwise heterotrophic bacteria, including *Sphingopyxis alaskensis*. The estimated H₂-derived cell-specific power was 5.4 × 10⁻¹³ W. Hydrogenase genes occurred across eight bacterial phyla and were expressed in ocean metatranscriptomes. (lappan2023molecularhydrogenin pages 6-7, lappan2023molecularhydrogenin pages 1-2) ### Boundaries - **Versus chemolithoautotrophy:** both obtain energy from inorganic donors, but lithoautotrophs obtain biomass carbon primarily from CO₂/HCO₃⁻. Growth on H₂ plus CO₂ alone, for example, is not evidence for this trait. (zeng2021microorganismsfromdeepsea pages 9-11, zeng2021microorganismsfromdeepsea pages 12-13) - **Versus chemoorganoheterotrophy:** if an organic compound supplies both electrons/energy and biomass carbon, the phenotype is organoheterotrophic unless an inorganic donor makes a demonstrated energetic contribution. - **Versus mixotrophy:** “mixotrophy” is broader and inconsistently applied. It can include simultaneous organic-carbon assimilation and CO₂ fixation, or co-oxidation of organic and inorganic energy sources. Curate `METPO:1000648` only where organic carbon is the primary biomass source and inorganic oxidation contributes energy. - **Maintenance versus growth:** CO oxidation is common, but the 2023 marine analysis concluded that CO generally supported survival during organic-carbon starvation, whereas H₂ produced enough power to support growth. CO oxidation alone should therefore not automatically imply lithoheterotrophic growth. (lappan2023molecularhydrogenin pages 6-7, lappan2023molecularhydrogenin pages 2-3) - **Genotype versus phenotype:** `coxL`, hydrogenase, `sqr`, or `sox` genes indicate potential, not the complete trait. Expression, donor consumption, acceptor reduction, growth/yield, and organic-carbon assimilation provide stronger evidence. - **Facultative status:** an organism can be lithoheterotrophic only under particular conditions and organoheterotrophic or lithoautotrophic under others. The graph should represent the assayed condition rather than impose an obligate lifestyle. ## 2. Candidate graph nodes ### Trait and process nodes - lithoheterotrophic — **“METPO:1000648”** - inorganic electron-donor oxidation - organic-carbon assimilation - aerobic respiration — `GO:0009060` - nitrate respiration — `GO:0042126` - denitrification — `GO:0019333` - hydrogen oxidation - carbon-monoxide oxidation - sulfide oxidation - thiosulfate oxidation - acetate assimilation - respiratory electron-transfer chain - proton-motive-force generation - ATP synthesis coupled to electron transport — `GO:0042773` - cellular growth — `GO:0016049` ### Chemicals and environmental inputs Conservative ChEBI candidates include: - molecular hydrogen — `CHEBI:18276` - carbon monoxide — `CHEBI:17245` - carbon dioxide — `CHEBI:16526` - dioxygen — `CHEBI:15379` - nitrate — `CHEBI:17632` - nitrite — `CHEBI:16301` - hydrogen sulfide — `CHEBI:16136` - thiosulfate — `CHEBI:26977` - elemental sulfur — label-only pending choice of the intended sulfur allotrope/species - iron(II) — `CHEBI:29033` - acetate — `CHEBI:30089` - glucose — `CHEBI:17234`
Curation history
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SEEDED_FROM_METPO · seed_from_metpo
imported from data/raw/metpo.owl (CLASS)
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ADDED_CAUSAL_GRAPH · codex
Added DOI-backed causal graph for inorganic electron donor oxidation, Fe(II), respiratory energy conservation, organic carbon use, and biomass formation.
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GROUND_CAUSAL_PREDICATES · claude
Grounded 3 causal-edge predicate_id field(s) via mappings/predicate_grounding.tsv (METPO:2000009×1, METPO:2000202×1, METPO:2000006×1).
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GROUND_CAUSAL_PREDICATES · claude
Grounded 2 causal-edge predicate_id field(s) via mappings/predicate_grounding.tsv (rdfs:subClassOf×2).
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GROUND_CAUSAL_PREDICATES · claude
Grounded 2 causal-edge predicate_id field(s) via mappings/predicate_grounding.tsv (METPO:2007402×1, METPO:2007403×1).
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GROUND_CAUSAL_NODES · claude
Grounded 3 causal-node grounding field(s) via mappings/node_grounding.tsv (CHEBI:29033×1, CHEBI:50860×1, GO:0022904×1).
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GROUND_CAUSAL_NODES · claude
Grounded 2 causal-node grounding field(s) via mappings/node_grounding.tsv (METPO:1007502×1, METPO:1007501×1).
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RETYPE_CAUSAL_NODES · claude
Re-typed 1 causal-node node_type field(s) to align with CausalNodeTypeEnum semantics: biomass: BIOLOGICAL_PROCESS → CHEMICAL ×1.
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GROUND_CAUSAL_PREDICATES · claude
Grounded 1 causal-edge predicate_id field(s) via mappings/predicate_grounding.tsv (biolink:part_of×1).
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ENRICH_CAUSAL_GRAPH · claude
Added 8 evidence-backed generic edges (8 new nodes) from the deep-research report.
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GROUND_CAUSAL_PREDICATES · claude
Grounded 6 causal-edge predicate_id field(s) via mappings/predicate_grounding.tsv (rdfs:subClassOf×2, METPO:2000016×2, METPO:2007402×1, RO:0002327×1).
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GROUND_CAUSAL_NODES · claude
Grounded 2 causal-node grounding field(s) via mappings/node_grounding.tsv (CHEBI:15138×1, CHEBI:16094×1).
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GROUND_CAUSAL_NODES · claude
Grounded 1 causal-node grounding field(s) via mappings/node_grounding.tsv (GO:0070224×1).
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REVERSE_CAUSAL_EDGE_DIRECTION · claude
Reversed 1 causal edge from <trait> uses electron donor <chemical> to <chemical> enables <trait> (predicate_id METPO:2000009 -> RO:0002327), issue 295. METPO:2000009 is rdfs:subPropertyOf METPO:2000001, whose rdfs:domain is METPO:1000525 (microbe), so the trait-subject form entailed that this TRAIT node is a microbe; CausalNodeTypeEnum has no organism member, so no causal-graph edge can satisfy that domain. Evidence unchanged; only subject/predicate/object/predicate_id and the edge description moved. Note RO:0002327 has range 'biological process or activity', so the new form is not fully range-correct either - tracked in issue 302.
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MIGRATE_ENABLES_TRAIT_EDGES · claude
Migrated 1 causal edge(s) off enables/RO:0002327 with a TRAIT object (1 to has electron donor), issue 302. RO:0002327 has range 'biological process or activity', which a trait (a disposition) cannot satisfy, so the previous form entailed trait is-a BiologicalProcessOrActivity. The replacements are proposed in proposals/metpo_traitmech_v8 and are placeholder ids until METPO mints them. 1 electron edge(s) were also reversed back to trait -> chemical, restoring the donor/acceptor role that PR 300 collapsed onto enables (issue 303); the organism-subject problem that forced that collapse does not arise here because these predicates take a causal-node domain rather than METPO:2000001's microbe domain (issue 301).
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MIGRATE_MICROBE_DOMAIN_EDGES · claude
Re-grounded 2 causal edge(s) off microbe-domain METPO predicates (1 to has output, 1 to has carbon source), issue 301. The previous predicates are transitively rdfs:subPropertyOf METPO:2000001, whose rdfs:domain is METPO:1000525 (microbe), so a causal-graph subject entailed that the subject IS a microbe; CausalNodeTypeEnum has no organism member, so no such edge could ever satisfy the domain. Edge directions are unchanged - this pass only relabels and re-grounds. RO:0002234 (has output) is used where the subject is an activity, since biolink gives it the domain 'biological process or activity'; the METPO replacements are proposed in proposals/metpo_traitmech_v8 and v9 and are placeholder ids until METPO mints them.
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MIGRATE_MICROBE_DOMAIN_EDGES_PART2 · claude
Re-grounded 2 causal edge(s) off microbe-domain METPO predicates onto their causal-graph counterparts (2 to oxidizes), issue 301 part 2. The previous predicates are transitively rdfs:subPropertyOf METPO:2000001, whose rdfs:domain is METPO:1000525 (microbe), so a causal-graph subject entailed that the subject IS a microbe; CausalNodeTypeEnum has no organism member, so no such edge could ever satisfy the domain. Each replacement is a 1:1 mirror of its source predicate that changes only the domain, so the claim each edge makes is unchanged and directions are unchanged. The replacements are proposed in proposals/metpo_traitmech_v9 and are placeholder ids until METPO mints them.
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NORMALISE_NODE_SENSE · claude
One node_id per SENSE (issues 356, 384): molecular_oxygen is the chemical sense here. The molecule, not the condition — the dioxygen participating in the reaction the graph describes. Normalised onto molecular_oxygen, the id 20 other chemical occurrences already use, so one id means one sense corpus-wide (issues 356, 384).